
mineral
Turquoise
CuAl6(PO4)4(OH)8·4H2O
Hardness: 5 to 6 on Mohs scale. Color: Robin's-egg blue to sky blue, blue-green, and apple green. Luster: Waxy to subvitreous or dull. Crystal Structure: Triclinic (rarely forms distinct crystals, usually microcrystalline or massive). Specific Gravity: 2.6 - 2.9.
- Hardness
- 5 to 6 on Mohs scale
- Color
- Robin's-egg blue to sky blue, blue-green, and apple green
- Luster
- Waxy to subvitreous or dull
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Physical properties
Hardness: 5 to 6 on Mohs scale. Color: Robin's-egg blue to sky blue, blue-green, and apple green. Luster: Waxy to subvitreous or dull. Crystal Structure: Triclinic (rarely forms distinct crystals, usually microcrystalline or massive). Specific Gravity: 2.6 - 2.9.
Formation & geological history
Formed by secondary or supergene enrichment processes when acidic, copper-rich circulating groundwater reacts with aluminum and phosphorus-bearing minerals in arid regions.
Uses & applications
Highly valued as an ornamental gemstone, used extensively in Native American and Middle Eastern jewelry, carvings, beads, and decorative lapidary arts.
Geological facts
Turquoise is one of the oldest known gemstones, mined since at least 6000 BCE in the Sinai Peninsula. The name comes from the French 'turquois', meaning 'Turkish', as it was originally brought to Europe via trade routes through Turkey.
Field identification & locations
Identified by its distinctive turquoise-blue color, opaque body, waxy luster, and often dark brown or black matrix veining. Major sources include the Southwestern United States (Arizona, Nevada), Iran (Persia), China, and Egypt.
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